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86Sr ratios displayed by soil carbonate in this section may result from weathering input by Eocene limestone into the ancestral middle Indus River system. Evidence that the lower two-thirds of this section represents the ancestral Indus River are that paleocurrent directions are generally southward and that phyllite and metaquartzite grains with accessory garnet indicate a Himalayan source.
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86Sr weathering contribution would be to analyze mineral separates, as weathering of different minerals proceeds at different rates. The abundance of detrital carbonate in these samples (2 to 13%) and its much greater solubility as compared with any silicate mineral make a significant contribution from silicates unlikely.
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1842396138
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note
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We thank J. Cater, R. Adams, and D. Schelling for discussions, samples, and unpublished sedimentological data from the Panir section; LASMO Oil Pakistan Ltd. and the Director General of Petroleum Concessions for provision of samples and permission to publish data from the Panir section; the Department of Soil Conservation in Babar Mahal, Kathmandu; and C. France-Lanord and L. Derry for discussions and access to unpublished data. The early stages of this research were supported and encouraged by M. McCulloch and A. Chivas at Australian National University. This project was primarily funded by NSF grant EAR-9418207.
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